Volume, Freshwater, and Heat Fluxes through Davis Strait, 2004-05

被引:125
作者
Curry, B. [1 ]
Lee, C. M. [1 ]
Petrie, B. [2 ]
机构
[1] Univ Washington, Appl Phys Lab, Seattle, WA 98105 USA
[2] Bedford Inst Oceanog, Ocean Sci Div, Dartmouth, NS, Canada
基金
美国国家科学基金会;
关键词
NORTH-ATLANTIC; VARIABILITY; OCEAN; ICE; CIRCULATION; SEA;
D O I
10.1175/2010JPO4536.1
中图分类号
P7 [海洋学];
学科分类号
0707 ;
摘要
Davis Strait volume [-2.3 +/- 0.7 Sv (1 Sv equivalent to 10(6) m(3) s(-1)); negative sign indicates southward transport], freshwater (-116 +/- 41 mSv), and heat (20 +/- 9 TW) fluxes estimated from objectively mapped 2004-05 moored array data do not differ significantly from values based on a 1987-90 array but are distributed differently across the strait. The 2004-05 array provided the first year-long measurements in the upper 100 m and over the shelves. The upper 100 m accounts for 39% (-0.9 Sv) of the net volume and 59% (-69 mSv) of the net freshwater fluxes. Shelf contributions are small: 0.4 Sv (volume), 15 mSv (freshwater), and 3 TW (heat) from the West Greenland shelf and -0.1 Sv, -7 mSv, and 1 TW from the Baffin Island shelf. Contemporaneous measurements of the Baffin Bay inflows and outflows indicate that volume and freshwater budgets balance to within 26% and 4%, respectively, of the net Davis Strait outflow. Davis Strait volume and freshwater fluxes nearly equal those from Fram Strait, indicating that both are significant Arctic freshwater pathways.
引用
收藏
页码:429 / 436
页数:8
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